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  1. Volcanic eruptions can produce ash particles with a range of sizes and morphologies. Here we morphologically distinguish two textural types: Simple (generally smaller) ash particles, where the observable surfa...

    Authors: Kimberly Genareau, Gopal K Mulukutla, Alexander A Proussevitch, Adam J Durant, William I Rose and Dork L Sahagian
    Citation: Journal of Applied Volcanology 2013 2:4
  2. Mapping the transport and deposition of tephra is important for the assessment of an eruption’s impact on health, transport, vegetation and infrastructure, but it is challenging at large distances from a volca...

    Authors: John Alexander Stevenson, Susan C Loughlin, Anna Font, Gary W Fuller, Alison MacLeod, Ian W Oliver, Ben Jackson, Claire J Horwell, Thor Thordarson and Ian Dawson
    Citation: Journal of Applied Volcanology 2013 2:3
  3. A new database of volcanic fatalities is presented and analysed, covering the period 1600 to 2010 AD. Data are from four sources: the Smithsonian Institution, Witham (2005), CRED EM-DAT and Munich RE. The data...

    Authors: Melanie Rose Auker, Robert Stephen John Sparks, Lee Siebert, Helen Sian Crosweller and John Ewert
    Citation: Journal of Applied Volcanology 2013 2:2
  4. Tephra fall is a major volcanic hazard and deposit characteristics are critical data used to quantify eruptive material. The homemade ashmeter is a device used to precisely measure thickness, area density, and...

    Authors: Benjamin Bernard
    Citation: Journal of Applied Volcanology 2013 2:1
  5. High risk volcanic events are commonly preceded by long periods of unrest during which scientists are asked to provide near real-time forecasts. The rarity of such events, inaccessibility of the underground vo...

    Authors: Jacopo Selva, Warner Marzocchi, Paolo Papale and Laura Sandri
    Citation: Journal of Applied Volcanology 2012 1:5
  6. To facilitate the assessment of hazards and risk from volcanoes, we have created a comprehensive global database of Quaternary Large Magnitude Explosive Volcanic Eruptions (LaMEVE). This forms part of the larg...

    Authors: Helen Sian Crosweller, Baneet Arora, Sarah Krystyna Brown, Elizabeth Cottrell, Natalia Irma Deligne, Natalie Ortiz Guerrero, Laura Hobbs, Koji Kiyosugi, Susan Clare Loughlin, Jonathan Lowndes, Martin Nayembil, Lee Siebert, Robert Stephen John Sparks, Shinji Takarada and Edward Venzke
    Citation: Journal of Applied Volcanology 2012 1:4
  7. Probabilistic modeling of lava flow hazard is a two-stage process. The first step is an estimation of the possible locations of future eruptive vents followed by an estimation of probable areas of inundation b...

    Authors: Laura J Connor, Charles B Connor, Khachatur Meliksetian and Ivan Savov
    Citation: Journal of Applied Volcanology 2012 1:3
  8. Human and livestock evacuation during volcanic crises is an essential component of volcanic risk management. This study investigates the evacuation of human and livestock populations from areas impacted by ash...

    Authors: Thomas Wilson, Jim Cole, David Johnston, Shane Cronin, Carol Stewart and Andre Dantas
    Citation: Journal of Applied Volcanology 2012 1:2

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